|

Executive Summary
The Problem
During
a typical winter, many areas in the Upper Midwest experience the problem
of blowing and drifting snow on roads and highways. The end result of
the problem often includes a reduction in driver safety, degradation of
road quality, and significant removal costs for drifted snow. Slick roads
and poor visibility caused by blowing and drifting snow result in hazardous
driving conditions. For example, from 1984 - 2001 there were 487 fatalities
during the months of November - March due to snow, severe winds and blowing
snow. Road quality can degrade due to the scraping of roadways and water
infiltration induced by snowmelt. Furthermore, significant snow removal
costs can be incurred by plowing and replowing windblown snow, not to
mention secondary revenue impacts such as shipping delays, reduced commerce,
lost salaries, and lost tax revenue.
The topography, land-use characteristics
and winter climate of western and southern Minnesota cause this area to
be particularly vulnerable such that blowing and drifting snow is a common
occurrence. The number of days with potential problems ranges from 115
in the south to 155 in the north. For an average winter season, taxpayers
in Minnesota spend approximately $100 million in snow removal costs, with
Mn/DOT expending $41 million. In the event of a winter season with anomalously
high snowfall and exceedingly strong winds, as was the case for much of
the state during the winter of 1996-97, the cost of snow removal can soar
to $215 million.
The Solution
Research
conducted in the 1960's and 70's by the U.S. Forest Service has shown
that snow fences cause blowing snow to deposit on the landscape such that
it is stored over the winter season. In the early 1970's, construction
for Interstate 80 was completed in eastern Wyoming, however, the highway
was subject to numerous drifting problems. Ronald Tabler and others utilized
this as an opportunity to apply research results and deploy structural
snow fences at problem locations along the interstate and test their effectiveness
as snow control measures. It is estimated that these snow fences prevented
35 accidental injuries and cut winter maintenance costs in half for one
season. Through these research efforts, detailed guidelines were established
by Tabler (1994) outlining the steps necessary for the deployment
of snow fences, both structural and living.
The Minnesota Department of Transportation
chose to utilize the technique for site specific snow control and one
study estimated that there are 4,000 sites, encompassing 1,000 miles,
where blowing and drifting snow is problematic (Gullickson 1999). When
comparing the cost of snow removal with living snow fences, an average
cost/benefit ratio of 17:1 exemplifies the efficiency of this method validating
widespread use in Minnesota. A research project was initiated by Mn/DOT
and conducted in collaboration with the University of Minnesota's Department
of Soil, Water, and Climate and the Minnesota State Climatology Office
(DNR - Waters). Subsequently, a technical advisory panel was formed consisting
of Mn/DOT, University of Minnesota and USDA-NRCS affiliates.
Climatological Research
Before
a blowing snow problem can be solved, several climatological factors in
the area of interest must be investigated. Climatological records of snowfall,
precipitation and temperature were compiled and archived in digital format
for all observing stations in Minnesota. This database represents the
climatic history of 370 locations throughout the state, some dating to
the 1850's. This represents the most spatially and temporally comprehensive
database available. In addition, wind speed and direction data from airport
observing stations in Minnesota and surrounding areas were also compiled.
With these data in hand, the climatological
parameters needed to design a living snow fence were computed. A knowledge
of three attributes is required, length of the snow season, snowfall during
that season, and the potential snow transport.
To define the first attribute, a method based
on mean monthly temperature was used, as described by Tabler (1994). This
allowed for the calculation of the beginning and ending dates of the snow
accumulation season across Minnesota. Secondly, the mean and frequency
distribution for snowfall during the snow season was determined. Finally,
to calculate potential snow transport, a set of models was utilized. The
snowfall and wind data, along with the precipitation data (used to determine
snow water equivalent), allowed for calculating the potential snow transport
Living Snow Fences in Minnesota
Since
snow fences are most often deployed on land used for crop production,
agricultural implications represent a chief concern for landowners. For
the winter of 2000-01, three locations in southern Minnesota, representing
three types of living snow fence designs, were studied. Each fence (previously
planted) was intended to protect a known problem section of highway.
-
Two 8-row strips of corn (planted
spring of 2000) placed 150-ft apart were left standing in a field
north of Gaylord, MN in Sibley County to protect a portion of Trunk
Highway 22. The landowner was compensated through Mn/DOT's standing
corn row program at a rate of $2.75 per bushel for the estimated number
of bushels of corn left standing in the field.
-
A twin-row 1998 planting of honeysuckle
protects Highway 14 just west of Lamberton, MN in Redwood County.
This fence was planted cooperatively by the University of Minnesota,
Mn/DOT, Redwood Soil and Water Conservation District and the Natural
Resource Conservation Service.
-
North of Mountain Lake, MN in
Cottonwood County, a section along Highway 30 proved to be a continuous
problem for travelers as well as the nearby landowner that often came
to the rescue for vehicles stuck in the snow. An alternating honeysuckle
and red cedar single living snow fence was planted 300-ft from the
north side of this highway in 1998.
Several features of the impacts of living snow fences
were investigated. Snow storage was measured at the end of the snow
season, which allowed for estimating the total volume of water that
was caught and stored at each fence. Soil temperature and the depth
to freezing was measured and studied in relation to snow depth. Soil
moisture was sampled adjacent to each fence after snowmelt to investigate
spatial variability, and finally a crop yield analysis was performed
for areas surrounding each fence that were affected by increased snow
deposition. The winter of 2000-01 proved to be an excellent season for
this type of research because the total snowfall amount ranked in the
highest 5% at these locations out of the last 100 years.
Key Findings
Task 1
-
The climatological database that
was compiled represents the best spatial and temporal coverage possible
for Minnesota.
-
The user is able to access daily
climatological records of temperature, precipitation and snowfall
for all available stations in Minnesota back to 1891.
-
During the 20th century, the annual
snowfall in Minnesota has increased an average of 1.5" per decade;
therefore it is advised that the mean snowfall for the most recent
30 year period (1971 - 2000) be incorporated in the snow transport
model when designing a living snow fence.
-
Analysis of hourly wind observations
showed that the predominant winter wind direction and the direction
of greatest snow transport may not be consistent, and the latter should
be utilized for snow fence design purposes.
-
New wind-blown snow relocation
coefficients have been calculated for Minnesota and are shown to vary
geographically with higher values in western portions of the state.
These values should be used in the mean seasonal snow transport model,
which helps the user determine the appropriate fence design.
-
The three living snow fence designs
performed exceptionally well for the near record-setting winter of
2000-01, storing 50% of their theoretical capacity (based on an empirically
developed equation using data from structural fences, Tabler 1994)
and protecting their respective roadways from drifted snow.
-
Given the high snow storage at
each fence and record-setting rainfall during and after snowmelt,
there was a relatively minor influence on crop yields adjacent to
the snow fences.
-
A 10' wide, black geotextile fabric
("EarthMat") was placed on top of the soil surface at Lamberton to
help establish the honeysuckle plantings. Comparative soil temperature
measurements at a 2" depth beneath the fabric and bare soil showed
that maximum daily temperatures in summer were lower under the fabric,
suggesting high heat loads were not a factor hindering survival of
new plantings.
-
A user is now able to view previously
unavailable snowfall and wind climatological products (Analysis
of Snow Climatology) and utilize these products to follow
the guidelines to design a living snow fence in an interactive, Web-based
environment (Case
Studies).
References
Gullickson, Dan et al. 1999.
Catching the Snow with Living Snow Fences. MN/DOT Office of Environmental
Services and University of Minnesota Extension Service (MI-7311-S) 140
pp.
Tabler, Ronald D., "Design
Guidelines for Control of Blowing and Drifting Snow", SHRP-H-381,
Strategic Highway Research Program, National Research Council, Washington,
D.C., 1994.
|